1) land-sea breeze
陆海风
2) land sea wind
海/陆风
3) sea and land breezes
海陆风
1.
By using a three dimensional meso-scale meteorological model based on the hydrostatic equilibrium which is modified to indude the effect of abrupt terrain, the daily evolution and three dimensional structure of sea and land breezes over Qingdao area are simulated.
本文采用 1个陡地形影响修正的三维中尺度流体静力的气象学模式 ,对青岛地区海陆风的日变化规律和三维结构进行了较细致的分析。
2.
The sea and land breezes over Hong Kong on 28 September 2004 was investigated with mesoscale model MM5.
利用MM5模式对香港地区的海陆风进行了显式数值研究,模拟的风向、风速和温度与站点的观测值比较一致,较详细地分析了海陆风的日变化规律和三维结构特征,结果显示香港地区海风分布复杂,主要受偏西、偏南和偏东海风气流的影响,形成多个辐合带,海风锋最远可以深入内陆约90km;陆风较简单,主要是偏北气流,陆风的风速和强度都比海风要弱,与山谷风、城市热岛环流等形成弱的辐合。
4) wind speed on land and sea
海陆风速
5) sea-land breeze
海陆风
1.
Some characteristics of sea-land breeze circulation over the coat of Hangzhou Bay;
杭州湾沿岸海陆风环流的若干特征
2.
Numerical simulation of three dimensional structure of sea-land breeze at west coast of Liao Dong Bay
辽东湾西岸三维海陆风特征的数值模拟
3.
Based on the boundary layer meteorological sounding and automatic meteorological station s data of Xinken on the west coast of the Pearl River mouth in October 2004,the characteristics of the sea-land breeze are studied.
根据2004年10月在珠江口西岸新垦观测的大气边界层探测资料和自动气象站资料,研究了珠江口西岸海陆风特征。
6) sea and land breeze
海陆风
1.
Analysis of the data observed from two automatic weather stations showed that the near surface wind field on the ice sheet was dominated by katabatic wind,while at seaboard a distinct feature is that this area was controlled by katabatic wind and sea and land breeze alternatively.
自动气象站(Automatic Weather Station,AWS)观测数据的统计分析结果表明,夏季该地区冰盖上的近表面风场主要是由下降风控制,而沿海地区的风场则由于海陆热力学性质的差异呈现出冰盖下降风与局地海陆风交互作用的特点。
补充资料：陆海
1.物产富饶之地。 2.南朝梁锺嵘对晋代文学家陆机有"陆才如海"之赞语。见《诗品》卷上。后因以"陆海"比喻富于文才。 3.借指陆机﹐以喻称富于文才的人。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条